High CO/H2 ratios supports an exocometary origin for a CO-rich debris disk
Abstract
Over 20 exocometary belts host detectable circumstellar gas, mostly in the form of CO. Two competing theories for its origin have emerged, positing the gas to be primordial or secondary. Primordial gas survives from the belt's parent protoplanetary disk and is therefore H2-rich. Secondary gas is outgassed in-situ by exocomets and is relatively H2-poor. Discriminating between these scenarios has not been possible for belts hosting unexpectedly large quantities of CO. We aim to break this gas origin dichotomy via direct measurement of H2 column densities in two edge-on CO-rich exocometary belts around 15 Myr-old A-type stars, constraining the COH2 ratio and CO gas lifetimes. Observing edge-on belts enables rovibrational absorption spectroscopy against the stellar background. We present near-IR CRIRES+ spectra of HD 110058 and HD 131488 which provide the first direct probe of H2 gas in CO-rich exocometary belts. We target the H2 (v=1-0 S(0)) line at 2223.3 nm and and the 12CO v=2→0 rovibrational lines in the range 2333.8-2335.5 nm and derive constraints on column densities along the line-of-sight to the stars. We strongly detect 12CO but not H2 in the CRIRES+ spectra. This allows us to place 3σ lower limits on the COH2 ratios of > 1.35 × 10-3 and > 3.09 × 10-5 for HD 110058 and HD 131488 respectively. These constraints demonstrate that at least for HD 110058, the exocometary gas is compositionally distinct and significantly H2-poor, compared to the <10-4 COH2 ratios typical of protoplanetary disks. We also find H2 alone is unlikely to shield CO over the lifetime of the systems. Overall this suggests that the gas in CO-rich belts is most likely not primordial in origin, supporting the presence of exocometary gas.
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